Abstract

Many studies quantify short-term drought impact on tree growth relative to pre-drought growth averages. However, fewer studies examine the extent to which droughts of differing severity differentially impact tree growth or shape stand dynamics. Focusing on three droughts in high and low density stands of Pinus sylvestris in Scotland, we calculated pre-drought growth averages using climatically standardized antecedent growth years to assess tree level drought and post-drought growth performance as percentage growth change (PGC). We then used mixed-effects models to understand how droughts of differing severity impact tree growth and calculated indices of growth dominance (Gd), size inequality (Si), and size asymmetry (Sa) to detect changes in stand structure. Mixed-effects model results indicate that the magnitude and duration of the growth reduction during and following the more extreme drought was significantly larger compared to less severe droughts, for which we found limited evidence of drought impact. While no changes in Si or Sa were noted following any drought, we found evidence of a difference in Gd after the most extreme drought in both stand densities indicative of a threshold response, with smaller trees contributing proportionally more to stand growth relative to their size. Under less severe droughts, inter-tree variability may have partially buffered against stand-level growth change, however, a small increase in drought severity was associated with a significant reduction in average tree growth, an increase in the number of trees growing at >2SD below pre-drought levels and a shift in Gd toward smaller trees, indicating that a drought severity threshold in P. sylvestris may have been exceeded.

Highlights

  • Climate change is expected to increase the frequency, intensity, and duration of extreme drought events globally (Shukla et al, 2019)

  • While the impact of all three drought events was more pronounced for spline detrended ring width data, the general patterns in percentage growth change (PGC) were the same as those derived from the basal area increments (BAI) analysis (Supplementary Figure 1)

  • In this study we developed a standardized method for calculating tree-level pre-drought growth averages using standardized precipitation evapotranspiration index (SPEI)-constrained growth years, against which drought and post-drought growth performance was assessed for three droughts of differing severity

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Summary

Introduction

Climate change is expected to increase the frequency, intensity, and duration of extreme drought events globally (Shukla et al, 2019). Increases in environmental stressors such as drought may potentially reshape species interactions away from competitive, toward more facilitative processes (He et al, 2013) These changes, coupled with the existence of nonlinear threshold-type responses to increasing drought severity (Cavin et al, 2013; Stuart-Haëntjens et al, 2015; Bartlett et al, 2016; Adams et al, 2017) means that understanding how and when drought alters forest structure and function (Haber et al, 2020) is increasingly important. If we are to implement successful forest management to promote stand-level drought resilience (Sohn et al, 2016), it is essential that we understand the interplay between increasing drought severity, patterns in forest response and the location of thresholds across a range of species, environments, and scales (Choat et al, 2012; Anderegg et al, 2015a; Huang et al, 2015)

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